Abstract
Modeling the pore system of carbonate rocks is not a simple task. Unlike sandstones that have a "homogeneous" pore system, carbonates exhibit a large range of pore types and pore throats with distinct sizes and morphologies (CHOQUETTE and PRAY, 1970; LUCIA, 1999; LØNØY 2006). This occurs due to a large range of factors such as the origin of the carbonate grains, sedimentary processes and …